EARTH S CHANGING SURFACE

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1 EARTH S CHANGING SURFACE

2 Weathering

3 Together, weathering and erosion work continuously to wear down the material on Earth s surface. weathering process that breaks down rock and other substances of Earth s surface erosion removal of rock particles by wind, water, ice or gravity

4 Weathering acts slowly, but over time will break down the largest and hardest of rocks mechanical weathering rock is physically broken down into smaller pieces by processes chemical weathering process that breaks down rocks through chemical changes

5 Mechanical Weathering Abrasion Rock particles wear away rock Freezing & Thawing Animal actions Plant growth Breaks rock by ice wedging Ground breaks away by animals burrowing Roots grow into cracks of rocks and pry them apart

6 Chemical Weathering Acid Rain Carbonic Acid Living Organisms Oxygen Results from burning fossil fuels causing minerals to wear away rapidly Forms from CO 2 dissolving in water then weathers marble and limestone Plants produce weak acid that slowly dissolve rock that surround roots Oxidation produces rust on some rocks that have iron

7 Important factors that determine the rate at which weathering occur are: climate refers to the average weather conditions in an area; both types of weathering occur faster in wet climates type of rock some minerals dissolve faster than others

8 Soil Formation

9 Soil formation bedrock solid layer of rock beneath the soil; once exposed bedrock gradually weathers in smaller particles that are the basic material of soil soil loose mixture of rock particles, minerals, decayed organic material, air and water in which plants can grow

10 Soil formation humus dark colored substance in soil from decayed organic material fertility measure of how well soil supports plant growth loam soil that is made up of equal parts of clay, sand, and silt; best for growing most types of plants

11 Soil formation continues over a long period and gradually develops layers called horizons. Cross section of soil showing horizons.

12 Soil formation continues over a long period and gradually develops layers called horizons. topsoil the A horizon or the top layer is crumbly, dark brown mixture of humus, clay and other mineral subsoil the B horizon in below topsoil consisting of clay and other particles washed down from top soil, but little humus C horizon bottom layer containing partly weathered rock

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14 Soil conservation management of soil to prevent its destruction contour plowing farmers plow their fields along the curves of the slope to help slow runoff of excess rainfall, which may wash away the soil conservation plowing farmers leave dead weeds and stalks of previous year s crops to all return nutrients to the soil, retain moisture and hold the soil in place crop rotation farmer plants different crops in a field each year

15 Erosion & Deposition Water and Wind

16 Water Erosion & Deposition Moving water is a major agent of erosion, especially along streams, rivers, at beaches, and underground. stream active water channel that erodes land and transports sediment river form on steep mountain slopes

17 Rivers form a variety of features: waterfalls occur where a river meets an area of rock that erodes slowly flood plains flat, wide area of land along a river that is often covered when the river overflows during a flood meanders loop-like bend in the course of a river and becomes more curved over time oxbow lakes meander that has been cut off from sediments being deposited and damming up the ends delta sediment deposited where a river flows into an ocean or lake and builds up a landform

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19 groundwater underground water that can cause erosion through a process of chemical weathering forming caves stalactite formed from deposits in dripping groundwater that hang on the roof of a cave stalagmite formed through deposits that build up a cone-shape on the cave floor

20 waves shape the coastlines through erosion by breaking down rock and transporting sand and other sediment; erode land by impact of great force and abrasion, or grinding away at shore beach area of deposited sediment carried in by a wave

21 Wind Erosion and Deposition Wind causes erosion by deflation, or the process by which wind removes surface materials and abrasion. Two common types of wind-blown deposits are dunes, piles of wind-blown sand and loess, or a crumbly, windblown deposit of silt and clay

22 Erosion & Deposition: Mass Movement and Glaciers

23 Erosion erosion process by which natural forces move weathered rock and soil, or sediment, from one place to another Factors that effect rate of erosion weather climate topography type of rock

24 Deposition deposition the laying down or settling of eroded material

25 Mass Wasting mass wasting downhill movement of a large mass of rocks or soil because of the pull of gravity (examples include: landslides, mudslides, slump and creep)

26 Glacier glacier large mass of ice that formed on land and moves slowly across Earth s surface; form in areas where the amount of snowfall is greater than the amount of snowmelt continental glacier (or ice sheets) covers large areas of land and move outward from central location; exist today on Antarctica and Greenland valley glacier (alpine) long, narrow glacier that forms when snow and ice build up high in a mountain valley

27 How Glaciers Shape the Land Two processes by which glaciers erode the land and plucking and abrasion. plucking occurs when a glacier flows over the land, it picks up rocks and large boulders dragging them across the land, causing abrasions, or gouges and scratches in the bedrock

28 Glacial Depositions When a glacier melts, it creates various landforms which include: till mixture of sediment that is deposited directly on the surface moraine ridge formed from till deposited at the edge of glaciers kettle small depression that forms when a chunk of ice is left in till then eventually melts

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